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RHex is an autonomous hexapedal robot capable of locomotion on rough terrain. Up to now, most modelling and simulation efforts on RHex were based on the linear leg assumption. These models disregarded what might be seen as the most characteristic feature of the latest iterations of this robot: the half circular legs. This thesis focuses on developing a more realistic model for this specially shaped compliant leg and studying its effects on the kinematics and dynamics of the resulting platform. One important consequence of the half circular compliant leg is the resulting rolling motion. Due to rolling, the rest length of the leg changes and the leg-ground contact point moves. Another consequence is the varying stiffness of the legs due to the changing rest length. These effect the resulting behaviour of any platform using these legs. In the first part of the thesis we are studying the effects of the half circular leg morphology on the kinematics of RHex using a simple planar model. The rest of the studies within the scope of this thesis focuses on the effect of the half circular compliant legs on the dynamics of a single legged hopping platform with a point mass. The formulation derived in this work is successfully integrated in a readily working but rather simple model of a single legged hopping system. We replace the equations of the straight leg in this model by the equations of the half circular compliant leg. Realistic results are obtained in the simulations and these results are compared to those obtained by the simpler constant stiffness straight leg model. This more realistic leg model brings us the opportunity to further study the effects of this leg morphology, in particular the positive effects of the resulting rolling motion on platform stability.

Made available in DSpace on 2014-06-11T19:28:33Z (GMT). No. of bitstreams: 0 Previous issue date: 2008-12-16Bitstream added on 2014-06-13T20:37:37Z : No. of bitstreams: 1 silvaneto_am_me_guara.pdf: 692597 bytes, checksum: 5f3caf79f195676ad932f7c214821ffc (MD5) / Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES) / O estudo de um modelo matemático completo, incluindo os servos atuadores, a dinâmica do corpo rígido e o planejamento e geração de trajetórias do manipulador robótico cilíndrico, é um indispensável ponto de partida para aplicações de simulação das juntas e controle de movimentos. As equações cinemáticas obtidas pelas técnicas da Matriz de Transformação Homogênea e Matriz de Transformação Inversa são a solução para a geração de trajetórias, as quais podem ser feitas no espaço cartesiano ou no espaço das juntas e também possibilitam gerar o volume de trabalho do manipulador, que é de grande interesse para a especificação de determinada configuração em aplicações ou tarefas específicas. As equações de movimento foram derivadas usando a formulação Lagrangiana para predizer o comportamento do manipulador quanto à influência da geometria e os parâmetros de massa do manipulador. / The study of a complete mathematical model including the servos actuators, the dynamics of the body rigid and the planning and generation of the manipulator's cylindrical robotic trajectories is an indispensable starting point for applications of simulation of the joints and control of movements. The Kinematic equations obtained by the techniques Homogeneous Transformation Matrix and Inverse Transformation Matrix make is the solution for generation of trajectories that can be done in the cartesian space or in the space of the joints and they also make possible to generate the volume of the manipulator's work that is of great interest for specification certain configuration in applications or specific tasks. The movement equations were derived using the formulation Lagrangiana to predict the manipulator's behavior as for the influence of the geometry and the parameters of the manipulator's mass.

Dizertační práce se zabývá problematikou kinematického modelování a řízení mobliních kolových robotů. Přináší sumarizaci problematiky kinematického modelování mobilních robotů obecně a popis vlastností kolových mobilních robotů s několika řízenými koly. Použitý aparát z matematiky, fyziky je vysvětlován s důrazem na pohled teorie řízení. Dále je prezentován nový řídicí algoritmus pro mobilní kolové roboty s více řízenými koly, vhodný pro úlohu stabilizace v bodě i sledování trajektorie, tedy obě nejčastěji řešené úlohy pohybu mobilních robotů.

Orogenic belts are fundamental features of plate tectonics. The crustal structure of orogens around the world shows a wide range of deformation styles from narrow, asymmetric wedges like the Pyrenees to wide, plateau-like orogens such as the Zagros or the Himalaya. The primary controlling factor on the size and structure of an orogen is the amount of convergence between the colliding plates. However, there are important additional factors providing major controls on the structural development of orogens. Among the potential parameters that can affect the style of deformation are the crustal strength, inherited weaknesses, and the surface processes. These parameters have been studied extensively in the past but their relative importance remains unclear. The aim of this thesis is to improve our understanding of: (1) How surface processes affect mountain building, with a special focus on the relationship between thin-skinned foreland and thick-skinned internal deformation of orogens. (2) How inherited extensional structures affect mountain building. The study was carried out using the Pyrenees as a special reference case. To answer our research questions we have used a wide range of state-of-the-art numerical modelling tools. In paper 1 we present a new method where we couple a structural-kinematic model and a thermo-kinematic model to evaluate the consistency of existing balanced section reconstructions with independent thermochronology data. In papers 2 and 3 we use 2D lithospheric scale thermo-mechanical models with surface process algorithms. Using the above toolset, we demonstrate that syntectonic sedimentation results in longer basement thrust sheets as well as longer thin-skinned thrust sheets and a generally wider orogen. Conversely erosion tends to narrow the wedge and reduce the orogenic loading of the colliding plates, limiting the space available for deposition in the flexural foreland deeps. We also demonstrate that inherited extensional structures play a crucial role in mountain building as they facilitate the migration of deformation into the undeformed basement of the overriding plate. Moreover, a significant amount of lower-crustal/mantle-lithospheric material is preserved at shallow depths only in the presence of extensional inheritance, but significant erosion is needed in order to bring this material to the surface. Our models also show that thin-skinned thrust sheets are generally rooted in the footwall of basement thrusts as they form outward-propagating sequences. As soon as a new basement thrust forms, the thin-skinned sequence situated on top of the new basement thrust-sheet is abandoned in favour of starting a new sequence in the footwall of the new thrust. Regarding our case study, it was possible to reproduce the section restoration using a structural-kinematic model with high accuracy up to the 36-Ma time slice and with limited accuracy up to the 50-Ma time slice. The thermochronometric ages predicted by the thermo-kinematic modelling are generally in good agreement with both the high- and low-temperature thermochronology data available in the Central Pyrenees; hence we conclude that the restoration is to a first order consistent with these datasets. The predicted thermochronological ages approximate the available low-temperature thermochronology data better by taking into account the late-stage burial and re-excavation scenario affecting the southern flank of the Pyrenean wedge presented by Coney et al. (1996), and quantified by Fillon and van der Beek (2012). In conclusion, our model experiments suggest, that extensional inheritance played a prime role in the structural evolution of the Pyrenees, with the major characteristics of the North Pyrenean Unit, including the presence of steep, inverted normal faults, the relative tectonic quiescence of the area after the early inversion and the presence of a lower-crustal body at shallow depth below the unit, best recaptured by our accordion models. / Orogenic belts are fundamental features of plate tectonics. The crustal structure of orogens around the world shows a wide range of deformation styles from narrow, asymmetric wedges like the Pyrenees to wide, plateau-like orogens such as the Zagros or the Himalaya. The primary controlling factor on the size and structure of an orogen is the amount of convergence between the colliding plates. However, there are important additional factors providing major controls on the structural development of orogens. Among the potential parameters that can affect the style of deformation are the crustal strength, inherited weaknesses, and the surface processes. These parameters have been studied extensively in the past but their relative importance remains unclear. The aim of this thesis is to improve our understanding of: (1) How surface processes affect mountain building, with a special focus on the relationship between thin-skinned foreland and thick-skinned internal deformation of orogens. (2) How inherited extensional structures affect mountain building. The study was carried out using the Pyrenees as a special reference case. To answer our research questions we have used a wide range of state-of-the-art numerical modelling tools. In paper 1 we present a new method where we couple a structural-kinematic model and a thermo-kinematic model to evaluate the consistency of existing balanced section reconstructions with independent thermochronology data. In papers 2 and 3 we use 2D lithospheric scale thermo-mechanical models with surface process algorithms. Using the above toolset, we demonstrate that syntectonic sedimentation results in longer basement thrust sheets as well as longer thin-skinned thrust sheets and a generally wider orogen. Conversely erosion tends to narrow the wedge and reduce the orogenic loading of the colliding plates, limiting the space available for deposition in the flexural foreland deeps. We also demonstrate that inherited extensional structures play a crucial role in mountain building as they facilitate the migration of deformation into the undeformed basement of the overriding plate. Moreover, a significant amount of lower-crustal/mantle-lithospheric material is preserved at shallow depths only in the presence of extensional inheritance, but significant erosion is needed in order to bring this material to the surface. Our models also show that thin-skinned thrust sheets are generally rooted in the footwall of basement thrusts as they form outward-propagating sequences. As soon as a new basement thrust forms, the thin-skinned sequence situated on top of the new basement thrust-sheet is abandoned in favour of starting a new sequence in the footwall of the new thrust. Regarding our case study, it was possible to reproduce the section restoration using a structural-kinematic model with high accuracy up to the 36-Ma time slice and with limited accuracy up to the 50-Ma time slice. The thermochronometric ages predicted by the thermo-kinematic modelling are generally in good agreement with both the high- and low-temperature thermochronology data available in the Central Pyrenees; hence we conclude that the restoration is to a first order consistent with these datasets. The predicted thermochronological ages approximate the available low-temperature thermochronology data better by taking into account the late-stage burial and re-excavation scenario affecting the southern flank of the Pyrenean wedge presented by Coney et al. (1996), and quantified by Fillon and van der Beek (2012). In conclusion, our model experiments suggest, that extensional inheritance played a prime role in the structural evolution of the Pyrenees, with the major characteristics of the North Pyrenean Unit, including the presence of steep, inverted normal faults, the relative tectonic quiescence of the area after the early inversion and the presence of a lower-crustal body at shallow depth below the unit, best recaptured by our accordion models.

MScEng / Thesis (MScEng (Mechanical and Mechatronic Engineering))--University of Stellenbosch, 2010. / ENGLISH ABSTRACT: Accurate dimensional measurement devices are critical for international industrial competitiveness for South Africa. An overview of all the necessary components of a laser tracking system using a multilateration technique for very accurate dimensional metrology is presented. A prototype laser tracker station was built to further investigate this type of system. The prototype successfully tracks a target within a volume of at least 200 200 200 mm3, approximately 300 mm away from the tracker. This system includes the mechanical design of a prototype tracker station, electronic implementation of ampli cation and motor control circuits, a tracking control algorithm, microcontroller programming and interfacing, as well as a user interface. Kinematic modelling along with Monte Carlo analyses nd the main error source of such a tracker as the beam steering mechanism gimbal axes misalignment. Multilateration is also motivated by the results found by the analysis. Furthermore, an initial sequential multilateration algorithm is developed and tested. The results of these tests are promising and motivate the use of multilateration over a single beam laser tracking system. / AFRIKAANSE OPSOMMING: Dit is van kritieke belang dat Suid-Afrika akkurate dimensionele metingstoestelle ontwikkel vir internasionale industriële medinging. 'n Oorsig van al die nodige komponente vir 'n Laser-Volgsisteem, wat slegs van multilaterasie gebruik maak om baie akkurate drie dimensionele metings te kan neem, word in hierdie projek voorgestel. 'n Prototipe Laser-Volgsisteem-stasie word gebou om so 'n sisteem verder te ondersoek. Die prototipe slaag wel daarin om 'n teiken, binne 'n volume van 200 200 200 mm3 op 'n afstand van omtrent 300 mm te volg. Die sisteem sluit die meganiese ontwerp van die sodanige stasie, elektroniese seinversterking, motorbeheer, 'n volgingsbeheer algoritme, mikroverwerker programeering en intergrasie, asook 'n gebruikerskoppelvlak program in. Kinematiese modelering, tesame met Monte Carlo simulasies, toon aan dat die hoof oorsaak van metingsfoute by so 'n stasie by die rotasie-asse van die laserstraal-stuurmeganisme, wat nie haaks is nie, lê. Die multilaterasie metode word ook verder ondersteun deur dié modelering. 'n Algoritme wat sekwensiële multilateratsie toepas word boonop ontwikkel en getoets. Die resultate van die toetse dui daarop dat die algoritme funksioneer en dat daar voordele daarin kan wees om so 'n metode in plaas van 'n Enkelstraal-Volgsisteem te gebruik.

The analogue models and the kinematic models based on the seismic data results were used to simulate the fault pattern which develops above a basement horst. The two major normal faults intersect with each other along the strike in the sedimentary covers. The fault pattern developed in the sedimentary cover is controlled by the dip of the basement fault and the width of the basement horst. The single horst structure was only developed in the sedimentary covers above the wider end of the basement horst. The hourglass structure was developed in the sedimentary covers above the narrower end of the basement horst. The precursor faults developed ahead of the major second-order normal faults when the dip angle of the basement fault is larger than 60°. The antithetic faults developed ahead of the major second-order normal faults when the dip angle of the basement fault is less than 50°. The analogue models were designed in a way that the two hanging wall blocks glide down along the basement horst simultaneously to simulate the activity of the basement faults. The kinematic models were designed based on the alternative sequential slip method to study the kinematic behaviors of the conjugate normal faults. The Lufeng Sag was characterized by the basement horst in the center and the deep half-grabens developed beside the horst. The width of the basement horst decreases along its strike. The models indicates that the second-order normal faults developed above the basement horst, observed in the Lufeng Sag seismic profiles, were reproducible and much more detailed structures were revealed / Detta projekt har analog modellering och kinematiska modeller baserade på seismiska data använts för att simulera förkastningsmönster ovanför en berggrundshorst. Två stora normal förkastningar möts i strykningsriktningen hos de ovanliggande sedimentlagren. Förkastningsmönstret som utvecklats i ovanliggande sedimentlager styrs av stupningen hos underliggande urberg samt bredden hos den underliggande horsten. Den enda horststrukturen som utvecklades i sedimentlagren skedde i fallet med en bredare underliggande horststruktur. En timglasstruktur bildades i den sedimentära successionen vid den smalare ändan av berggrundshorsten. De initiala förkastningarna bildades tidigt för att sedan övergå i andra ordningens normalförkastningar i de fall då stupningen hos underliggande berggrund överstiger 60°. Mindre antitetiska förkastningar bildades före andra ordningens förkastningar där berggrunds-stupningen understiger 50°. Den analoga modell som nyttjades experimentellt var konstruerad så att de två hängväggskomponenterna kunde röra sig fritt samtidigt längs med berggrundshorsten för att simulera aktivering av befintliga förkastningar i berggrunden. De kinematiska modeller som nyttjades var konstruerade enligt metoden för sekventiella rörelser (eng - sequential slip method) för att studera kinematiska beteenden hos konjugerande förkastningspar. Lufeng-sänkans utseende har kontrollerats av berggrundshorsten i mitten samt av de djupa halv-grabens på båda sidorna av horsten. Bredden på berggrundshorsten minskar längs dess stupning. Modellerna påvisar att andra ordningens normal-förkastningar bildades ovanför berggrundshorsten, likt i de seismiska profilerna över området, samt att strukturerna var reproducerbara och väldigt detaljrika.

The automation of the tramming or load, haul and dump (LHD) procedure, performed by a LHD vehicle, holds the potential to improve productivity, efficiency and safety in the mining environment. Productivity is mainly increased by longer working hours; efficiency is improved by repetitive, faultless and predictable work; and safety is improved by removing the human operator from the harsh environment. However, before the automation of the process can be addressed, a thorough understanding of the process and its duty in the overall mining method is required. Therefore, the current applicable mining methods and their areas of potential automation are given. Since the automation of the LHD vehicle is at the core of this project, its implementation in the tramming process is also justified. Also, the current underground navigation methods are given and their shortcomings are named. It is concluded that infrastructure-free navigation is the only viable solution in the ever-changing mining environment. With that in mind, the feasibility of various navigation sensors is discussed and conclusions are drawn. Both kinematic and dynamic modelling of LHD vehicles are introduced. Various forms of kinematic models are given and their underlying modelling assumptions are named. The most prominent assumptions concern the vehicle’s half-length and the inclusion of a wheel-slip factor. Dynamic modelling techniques, with a strong emphasis on tyre modelling, are also stated. In order to evaluate the modelling techniques, field tests are performed on the articulated vehicles, namely the Wright 365 LHD and the Bell 1706C loader. The test on the Wright 365 LHD gives a good impression of the harsh ergonomics under which the operator has to work. A more thorough test is performed on the Bell 1706C articulated loader. The test results are then compared to simulation results obtained from the kinematic models. Also, the above-named assumptions are tested, evaluated and discussed. A dynamic model is also simulated and discussed. Lastly, two localization and control methods are given and evaluated. The first method is an open-loop nonlinear optimal control strategy with periodic position resetting and the second method is a pathtracking controller. AFRIKAANS : Automatisering van die laai-, vervoer- en dompel- (LVD) prosedure het die potensiaal om die produktiwiteit, effektiwiteit en veiligheid van die mynbedryf te verbeter. Produktiwiteit word hoofsaaklik deur langer werksure verhoog, effektiwiteit word deur herhalende, foutlose en voorspelbare werk verbeter en veiligheid word verbeter omdat menslike operateurs uit die gevaarlike ondergrondse omgewing verwyder word. Voordat aandag aan die automatisering van die prosedure geskenk kan word, moet die prosedure en die algemene mynbedrywighede rakende die prosedure deeglik bestudeer en verstaan word. As gevolg hiervan word die huidige, toepaslike mynboumetodes hier gedokumenteer. Die implementering van ʼn gekoppelde LVD-voertuig in die LVD-prosesword ook geregverdig. Verder word die huidige metodes van ondergrondse navigasie genoem en hulle tekortkominge aangedui. Die gevolgtrekking dat infrastruktuur-vrye navigasie die enigste lewensvatbare navigasiemetode in die immer veranderende ondergrondsemynbouomgewing is, word ook gemaak. In die lig daarvan word ʼn verskeidenheid sensors genoem en bespreek. Kinematiese en dinamiese modellering van ʼn LVD-voertuig word bekendgestel. Verskeie kinematiese modelle en hulle onderliggende aannames word genoem. Die mees prominente aannames is die lengte van die gekoppelde voertuig se hoofdele en die insluiting van ʼn wielglipfaktor. Die tegnieke van dinamiese modellering, met die klem op bandmodellering, word ook gegee. Praktyktoetse op gekoppelde voertuie is ook gedoen om die verskillende modelle te evalueer. Die toets op die Wright 365-LVD bied goeie insig in die strawwe ergonomiese toestande waaronder die operateurs moet werk. ʼn Deeglike toets is op ʼn BELL 1706C- gekoppelde laaier, wat kinematies identies aan ʼn LVD-voertuig is, uitgevoer. Die bevindinge van die toets word met bogenoemde modelsimulasies vergelyk en gevolgtrekkings word gemaak. Laastens word lokalisiering en beheer van ʼn LVDvoertuig behandel. Twee beheermetodes, opelus- nie-lineêre optimale beheer met periodieke herstel en padvolgingbeheer word geëvalueer en bespreek. Copyright / Dissertation (MEng)--University of Pretoria, 2012. / Electrical, Electronic and Computer Engineering / unrestricted

Les Grès d’Annot préservés dans les chaînes subalpines méridionales sont des turbidites riches en sable déposées dans le basin d’avant pays alpin durant l’Eocène supérieur et l’Oligocène inférieur. La sédimentologie et la stratigraphie de ce système turbiditique ont déjà été étudiées, mais le contexte structural reste mal connu. Cette thèse est consacrée à l’étude tectonique des Grès d’Annot, combinant un travail de terrain et l’utilisation d’outils de modélisation géométrique en 3D (gOcad) et cinématique (Trishear), centrés sur les sous-bassins d’Annot, du Grand Coyer et de Sanguinière. L’objectif est d’étudier l’héritage et l’évolution structural du bassin turbiditique et de le replacer dans le contexte régional du SE de la France. Les résultats indiquent que le remplissage du bassin périalpin précoce (Eocène et Oligocène) est bien plus complexe qu’une simple migration de la sédimentation (Grès d’Annot) et de la déformation vers l’avant pays. Ils révèlent des interactions entre tectonique et sédimentation à différentes échelles. A l’échelle de l’avant-pays, une coupe équilibrée illustre le contrôle primordial de la marge passive salifère préexistante sur la structure de la chaîne plissée. Le sel triasique constitue un décollement basal régional, qui de par sa faiblesse, a accommodé une déformation alpine précoce d’une large zone de l’avant-pays dès l’Éocène moyen et supérieur. Les variations de stratigraphie mécanique des séries mésozoïques sont à l’origine d’un changement de style structural : lors de la compression, plusieurs niveaux de décollement actifs se développent dans la partie orientale où les séries sont plus argileuses et plus fines. Ceci induit, en surface, une géométrie de bassin complexe avec des plis de longueurs d’ondes différentes et des migrations de charnière au cours de la sédimentation turbiditique. L’héritage structural du bassin d’avant-pays, jusqu’alors sous-estimé, est le résultat de l’ouverture de la Téthys alpine et d’une déformation précoce régionale exprimée par des plis d’axe E-W qui débute dès le Crétacé supérieur et s’accentue durant l’Éocène moyen. Des résultats préliminaires de thermochronologie (datations U-Th/He sur zircons détritiques de grès moyens à grossiers ou de granodiorites présentes dans les coulées de débris du dépocentre de Sanguinière) suggèrent une exhumation des reliefs à l’origine du matériel détritique liée à cette déformation crétacée. L’étude structurale détaillée de la série des Grès d’Annot et de son substratum dans les sous-bassins d’Annot et du Grand Coyer permet de définir en 3D les connections entre les dépocentres et de proposer une évolution structurale de ceux-ci à l’échelle du bassin. Les paléocourants montrent un parallélisme avec la direction des plis majeurs, indiquant un confinement alors que des directions divergentes à proximité des structures tectoniques plus mineures ou transverses suggèrent que ces dernières interagissent avec les écoulements. Les turbidites se déposent parallèlement dans plusieurs synclinaux alpins, actifs en alternance ou en même temps. A l’échelle des dépocentres, la modélisation géométrique 3D du dépocentre d’Annot en utilisant gOcad permet d’identifier les structures héritées et de démontrer la contemporanéité du plissement alpin et des dépôts turbiditiques. La migration de l’onlap des dépôts de grès et la variation des pendages à l’intérieur des membres turbiditiques sont associées à une migration du dépocentre. Cette géométrie est liée à une migration de la charnière synclinale qui favorise une tendance des dépôts à migrer latéralement plutôt qu’à s’empiler.D’un point de vue sédimentologique et stratigraphique, les Grès d’Annot sont connus pour être un bon analogue des réservoirs des grands fonds de type « riches en sable », situés sur les marges passives en aval de deltas. / The Annot Sandstone, exposed in the southern sub-alpine chains, consists of sand-rich turbidites deposited in the Tertiary Alpine foreland basin (Upper Eocene – Lower Oligocene Annot Sandstone basin). While the sedimentology and stratigraphy of this turbidite system have been largely described and discussed, its structural framework remains unconstrained. This thesis presents a study of the tectonics of the Annot Sandstone basin based on field surveys and 3D geometrical (gOcad) and kinematic modelling (Trishear), focusing in particular on the Annot, Grand Coyer and Sanguinière sub-basins. Objectives were to determine the structural evolution of the sub-basins, including the role of inherited features, and to use these data to better constrain the alpine tectonic history of SE France.Infill of the early alpine foreland basin is more complex than a simple foreland migration of sedimentation and deformation. Results reveal complex interactions of tectonics and sedimentation at different scales during deposition of the Annot Sandstone.•At the foreland scale, a balanced cross-section illustrates the critical control by the pre-existing salt-based passive margin architecture on the structure of the fold and thrust belt. Triassic evaporates regionally acted as a weak basal detachment, accommodating an early alpine deformation phase of the whole foreland from the Middle to Upper Eocene. Variations in mechanical stratigraphy within the Mesozoic sediments generated a change in structural style. For example, the eastern region is characterized by a thinner, shalier Mesozoic succession, leading to several active detachments during alpine compression. Multiple fold wavelengths and synsedimentary rolling hinges generated by these active detachments led to complex depocentres. The previously under-estimated structural heritage of the foreland basin derived from rifting and spreading of the Alpine Tethys and from an early regional deformation responsible for E-W trending folds, which began in the Late Cretaceous and increased during the Middle Eocene. Preliminary thermochronology results (U-Th/He datings on detrital zircons of medium to coarse sandstone blocks and granodiorite blocks from debris flows of the Sanguiniere depocentre) suggest an exhumation of source areas during this Cretaceous deformation.•A detailed study of structures within the Annot and Grand Coyer sub-basins and their Cretaceous substrate revealed connected depocentres evolving in 3D at the basin scale. Paleocurrent directions are mainly parallel to the main alpine fold axes recording structural confinement, while some diverging directions indicate flow interaction with minor or oblique tectonic features. Turbidites were deposited along the axis into several alpine synclines, which were simultaneously or successively active.•Concerning the depocentre infill, 3D geometrical modelling of the Annot depocentre (using gOcad) was used to identify inherited structures and to constrain alpine fold activity during turbidite deposition. The onlap migration and the specific stacking and dip pattern within turbidite members (laterally rather than vertically stacked deposits) record depocentre migration linked with a rolling synclinal hinge. Due to its sedimentology and its stratigraphy, the Annot Sandstone is well-known as an analogue for sand-rich reservoirs deposited at delta toes in deep-water passive margins. This study reveals that, structurally, it is also a good example of axially-sourced turbidite depocentres developed on a multi-detachement fold and thrust belt